Tidal Effects on MFP Via the Intimate96 Test

2002 ◽  
pp. 457-463 ◽  
Author(s):  
A. Tolstoy ◽  
S. Jesus ◽  
O. Rodriguez
Keyword(s):  
Tidal Effects

scholarly journals From amplitudes to gravitational radiation with cubic interactions and tidal effects

2021 ◽  
Vol 103 (4) ◽  
Author(s):  
Manuel Accettulli Huber ◽  
Andreas Brandhuber ◽  
Stefano De Angelis ◽  
Gabriele Travaglini
Keyword(s):  
Gravitational Radiation ◽  
Tidal Effects

Tidal Effects on Determining a Point at the Bottom of the Sea by Combining GPS and Sonar Observations

2001 ◽  
Vol 24 (1) ◽  
pp. 35-51
Author(s):  
Wenke Sun, Lars E. Sjöberg
Keyword(s):  
Tidal Effects

Estimation and Removal of Tidal Effects From Pressure Data

SPE Journal ◽  
2009 ◽  
Vol 14 (01) ◽  
pp. 144-152 ◽  
Author(s):  
Yong Zhao ◽  
Albert C. Reynolds
Keyword(s):  
Pressure Data ◽  
Tidal Effects

Tidal effects in a spacecraft

2021 ◽  
Vol 89 (10) ◽  
pp. 909-915
Author(s):  
Ugo Besson
Keyword(s):  
Tidal Effects

Address of the President, Sir Howard Florey, at the Anniversary Meeting, 30 November 1964

1965 ◽  
Vol 283 (1392) ◽  
Keyword(s):  
Interplanetary Space ◽  
Diurnal Variations ◽  
Kinetic Theory Of Gases ◽  
Tidal Effects ◽  
Subsequent Work ◽  
The Earth ◽  
Predominant Component ◽  
Wide Range ◽  
Magnetic Field Variations ◽  
Great Mass

The Copley Medal is awarded to Professor S. Chapman, F.R.S. Professor Chapman is distinguished for his contributions to many aspects of physics, astronomy and geophysics. His work on the kinetic theory of gases now forms the basis for much detailed study of gaseous phenomena, and over forty years ago his interest in these problems led him to consider the processes of diffusion and viscosity in stars. In addition to these important studies Chapman’s name has, for over half a century, been inseparably linked with problems in terrestrial magnetism and with a wide range of studies concerned with the high atmosphere, ionosphere and interplanetary space. From a statistical analysis of a great mass of data Chapman succeeded in demonstrating the existence of a small lunar component in the Earth’s quiet magnetic field variations, and he showed that the solar and lunar diurnal variations could be separated into a predominant component originating above the Earth’s surface and a subsidiary component within the Earth itself. From this standpoint he developed the general theory of the relation of the magnetic variations to the solar and lunar atmospheric tidal effects, a theory which has been fundamental to all subsequent work.

scholarly journals Study on the Impact of Tidal Effects on Water Quality Modelling of Juru River, Malaysia

2011 ◽  
Vol 4 (2) ◽  
pp. 129-138 ◽  
Author(s):  
Mohd Ekhwan Toriman ◽  
Norbaya Hashim ◽  
Abd. Jalil Hassan ◽  
Mazlin Mokhtar ◽  
Hafizan Juahir ◽  
...  
Keyword(s):  
Water Quality ◽  
Tidal Effects ◽  
Water Quality Modelling ◽  
The Impact

scholarly journals Short-term tidal variations in UT1: compliance between modelling and observation

2009 ◽  
Vol 5 (H15) ◽  
pp. 215-215 ◽  
Author(s):  
Sigrid Englich ◽  
Harald Schuh ◽  
Robert Weber
Keyword(s):  
Solid Earth ◽  
Earth Tides ◽  
Time Interval ◽  
Observation Data ◽  
Length Of Day ◽  
Tidal Effects ◽  
Short Term ◽  
Solid Earth Tides ◽  
Oceanic Tides ◽  
Tidal Variations

AbstractThe Earth rotation rate and consequently universal time (UT1) and length of day (LOD) are periodically affected by solid Earth tides and oceanic tides. Solid Earth tides induce changes with periods from around 5 days to 18.6 years, with the largest amplitudes occurring at fortnightly, monthly, semi-annual and annual periods, and at 18.6 years. The principal variations caused by oceanic tides have diurnal and semi-diurnal periods. For the investigation of the tidal effects with periods of up to 35 days, UT1 series are estimated from VLBI observation data of the time interval 1984–2008. The amplitudes and phases of the terms of interest are calculated and the results for diurnal and sub-diurnal periods are compared and evaluated with tidal variations derived from a GNSS-based LOD time series of 8 months. The observed tidal signals are finally compared to the predicted tidal variations according to recent geophysical models.

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